1st Quarter Vocabulary
- Silicate mineral: a mineral that contains a combination of silicon, oxygen, and other elements
- Nonsilicate mineral: a mineral that does not contain compounds of silicon and oxygen
- Mineral: a naturally formed, inorganic solid that has a definite crystalline structure
- Element: a substance that cannot be separated or broken down into simpler substances by chemical means
- Mineral Physical Properties: Ways to identify specific minerals by luster, hardness, color, cleavage or fracture, streak, and special properties
- Metamorphic Rock: from other rocks because thermal heat and extreme pressure have been applied it changes the chemical makeup
- Igneous Rock: from the melted magma that has cooled and solidified
- Sedimentary Rock: from layers of sediment building up in oceans that compacted and cemented together
- Sediment: small pieces of rock and soil
- Weathering:Breaking rocks, mountains, or ground soil into pieces by wind, rain, or temperatures
- Erosion: process by which sediment is removed from its source to low places
- Deposition: the action of depositing, dropping material into piles and layers
- Foliated: in metamorphic rock when mineral grains are arranged in bands or patterns.
- Intrusive Igneous Rock: that cools deep in the Earth below the surface.
- Extrusive Igneous Rock: that cools as a result of volcanic activity throwing or seaping outside at the Earth’s surface
- Texture: size, shape, and position of grains that make up a rock looks
- Uplift: rising of rock layers at faults, Convergent Boundaries
- Normal fault: hanging wall moves down relative to footwall, Divergent Boundaries
- Reverse Fault: hanging wall moves up relative to footwall, Convergent Boundaries
- Sea-Floor Spreading: ocean floor splitting apart, divergent boundaries, at mid-ocean ridges, new oceanic crust forms
- Continental Drift: hypothesis that the continents were once one large mass, Pangea, that broke apart and drift around on the asthenosphere
- Fossils: Solidified remains of once living organisms that provide evidence that the continental drift
- Core: the layer of Earth made mostly of iron and nickel
- Inner Core: Solid, iron and nickel
- Outer Core: Liquid, iron and nickel
- Mantle: Molten rock, comprises 67% of Earth’s mass
- Crust: the thin, solid outermost layer above the mantle
- Asthenosphere: the layer made of gooey rock that slowly flows, tectonic plates float on
- Divergent Boundary: where two plates are moving away from each other
- Convergent Boundary: where two plates move towards each other and collide
- Transform Boundary: where two plates are moving horizontally past each other
- Convection Current: In the mantle, the raising of heated magma, and the sinking of cooler magma, the circular motion causes tectonic plates to move.
- Continental to continental convergent: folded mountains form
- Continental to oceanic convergent: subduction zone, volcanic mountains
- Oceanic to oceanic convergent: subduction zones
- Transform, strike-slip boundaries: Earthquakes
- Mid-Ocean Ridges: divergent boundaries in the ocean, new oceanic floor
- Valley Rifts: divergent boundaries on land
- Alfred Wegener: Continental Drift-proof - climate change residue, fossils, land formations
- Bioengineering: the application of applying engineering to living things
- Benefits: an advantage or profit gained from something
- Unintended consequences: results that were not planned for when creating a new product
- Prototype: a test model of a product
- Independent Variable: a variable whose variation does not depend on that of another, Changed by the scientist, Cause
- Dependent Variable: a variable whose value depends on that of another, Changes because of the ID, Effect
- Control Variable: Used to compare the results against
- Constance: All other factors in an experiment that stays the same.
- Volume: the amount in a given space, usually measured in liters
- Mass: The amount of matter something has , measured using kilograms